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Comparison of suitable drought indices for climate change impacts assessment over Australia towards resource management

机译:比较适用于澳大利亚气候变化影响评估的干旱指数对澳大利亚资源管理的影响

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Droughts have significant environmental and socio-economic impacts in Australia. This emphasizes Australia's vulnerability to climate variability and limitations of adaptive capacity. Two drought indices are compared for their potential utility in resource management. The Rainfall Deciles-based Drought Index is a measure of rainfall deficiency while the Soil-Moisture Deciles-based Drought Index is a measure of soil-moisture deficiency attributed to rainfall and potential evaporation. Both indices were used to assess future drought events over Australia under global warming attributed to low and high greenhouse gas emission scenarios (SRES BI and AIFI respectively) for 30-year periods centred on 2030 and 2070. Projected consequential changes in rainfall and potential evaporation were based on results from the CCCmal and Mk2 climate models, developed by the Canadian Climate Center and the Australian Commonwealth Scientific and Industrial Research Organisation (CSIRO) respectively. A general increase in drought frequency associated with global warming was demonstrated by both indices for both climate models, except for the western part of Australia. Increases in the frequency of soil-moisture-based droughts are greater than increases in meteorological drought frequency. By 2030 in the frequency of soil-moisture-based drought frequency increases 20-40% over most of Australia with respect to 1975-2004 and up to 80% over the Indian Ocean and southeast coast catchments by 2070. Such increases in drought frequency would have major implications for natural resource management, water security planning, water demand management strategies, and drought relief payments. Copyright (C) 2007 Royal Meteorological Society.
机译:干旱对澳大利亚的环境和社会经济产生重大影响。这强调了澳大利亚对气候变化的脆弱性和适应能力的局限性。比较了两个干旱指数在资源管理中的潜在效用。基于降雨十分位数的干旱指数是对降水不足的一种度量,而基于土壤湿度十分位数的干旱指数是对由于降雨和潜在蒸发引起的土壤水分不足的度量。两种指数均用于评估在全球变暖的情况下澳大利亚未来的干旱事件,这归因于2030年和2070年为期30年的低温室气体排放情景和高温室气体排放情景(分别为SRES BI和AIFI)。预计降雨和潜在蒸发的相应变化为基于分别由加拿大气候中心和澳大利亚联邦科学与工业研究组织(CSIRO)开发的CCCmal和Mk2气候模型的结果。除澳大利亚西部以外,这两个气候模型的两个指数均表明与全球变暖有关的干旱频率普遍增加。基于土壤水分的干旱频率的增加大于气象干旱频率的增加。到2030年,相对于1975-2004年,澳大利亚大部分地区基于土壤水分的干旱频率将增加20-40%,到2070年,印度洋和东南沿海流域的干旱频率将增加80%。这种干旱频率将增加对自然资源管理,水安全计划,水需求管理策略和抗旱救济金有重大影响。皇家气象学会(C)2007。

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